Colloidal
systems, including micellar and reverse micellar mixtures,
are essential for a variety of natural transport processes, such as
the flow of organic and inorganic contaminants in lakes, rivers, and
underground fissures. Thus, an understanding of their structure and
stability is important for prediction of their behavior in complex
environments. Previous experiments have shown that the solvodynamic
diameters (D) of reverse micelles contract linearly
with increased concentrations of salts such as NaBH4, FeSO4, Mg(NO3)2, CuCl2, Al(NO3)3, Fe(NO3)3, and Y(NO3)3. It has also been previously determined that
reverse micelle size is a function of cation valency, through the
Debye screening length (κ–1), and of anion
hydrated radius. Here, we present a new theoretical model for the
aqueous reverse micelle core substructure in water/AOT/isooctane colloidal
systems with added salts. Our model is based on electrical double
layer (EDL) theory and assumes ions are evenly distributed within
the reverse micelle water core. We further analyze reverse micelle
size with respect to ion hydration, reverse micelle water dynamics,
and ion distribution, to propose a mechanism for reverse micelle contraction
and determine the cause of system instability at the critical destabilization
concentration for each salt. We find that destabilization occurs when
the interfacial core water and waters needed for complete ion hydration
exceed the water contained within the reverse micelle at its stable
size. This establishes ion hydration capacity a likely primary mechanism
for reverse micelle destabilization.